fault lines
convergent plate boundaries
"plates" are the term for the giant sheets of rock on the earths crust
Tectonic plate boundaries are specific areas where the Earth's plates interact and move against each other, leading to seismic activity such as earthquakes. These boundaries can be categorized into different types based on the direction of the plate movement, such as convergent, divergent, and transform boundaries.
fault lines
The edges of continental plates are called fault lines because they are boundaries where tectonic plates meet and interact. These interactions can create faults, which are fractures within the Earth's crust where rocks have moved relative to each other. Fault lines are prone to seismic activity such as earthquakes due to the stress and movement along these boundaries.
QuestionThe term for the circular movement of material inside earth's mantle is convection current. This current causes the movement of the tectonic plates.
QuestionThe term for the circular movement of material inside earth's mantle is convection current. This current causes the movement of the tectonic plates.
QuestionThe term for the circular movement of material inside earth's mantle is convection current. This current causes the movement of the tectonic plates.
QuestionThe term for the circular movement of material inside earth's mantle is convection current. This current causes the movement of the tectonic plates.
The term is "orogenesis." It refers to the geological process of mountain building, typically occurring at convergent plate boundaries where tectonic plates collide, leading to the uplift of the Earth's crust and the formation of mountain ranges.
A rift boundary is a divergent boundary, where two plates of the earth's crust are moving away from each other. Divergent boundaries occur at mid-oceanic ridges on the sea floor, but usually the term rift is used to describe divergent boundaries on the land. The best known one is in eastern Africa.
The term "tectonic plate" refers to a large, rigid segment of the Earth's lithosphere, which is the outermost shell of the Earth. These plates are responsible for the movement and geological activity on the Earth's surface. Tectonic plates vary in size but can be enormous, covering vast areas of the Earth's surface. They float on the semi-fluid asthenosphere beneath them. The theory of plate tectonics explains how these plates interact with each other. It suggests that the Earth's lithosphere is divided into several major plates and numerous smaller ones, and these plates are in constant motion. The interactions between tectonic plates give rise to various geological phenomena, such as earthquakes, volcanic eruptions, mountain formation, and the creation of ocean basins. The boundaries between these plates are where a lot of these geological activities occur, and they are classified into different types, including divergent boundaries (where plates move apart), convergent boundaries (where plates move toward each other), and transform boundaries (where plates slide past each other horizontally). In essence, tectonic plates play a fundamental role in shaping the Earth's surface and are central to our understanding of Earth's geology and the processes that have shaped the planet over millions of years.